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德国土壤中的稀土元素——综述。

Rare earth elements in German soils - A review.

机构信息

University of Wuppertal, School of Architecture and Civil Engineering, Soil- and Groundwater-Management, Pauluskirchstraße 7, D-42285 Wuppertal, Germany.

University of Wuppertal, School of Architecture and Civil Engineering, Soil- and Groundwater-Management, Pauluskirchstraße 7, D-42285 Wuppertal, Germany; Sejong University, Department of Environment, Energy and Geoinformatics, 98 Gunja-Dong, Guangjin-Gu, Seoul, South Korea.

出版信息

Chemosphere. 2018 Aug;205:514-523. doi: 10.1016/j.chemosphere.2018.04.059. Epub 2018 Apr 12.

Abstract

Rare earth elements (REEs) are increasingly used in high-tech industry, agriculture, and healthcare technologies what leads to their release into soils and waters, and to the transfer into plants what may have negative impacts on human health and the environment. The toxicity and potential mobilization of REEs in soils can be assessed by their content and geochemical behavior along with soil properties. However, those interactions are so far not reviewed in German soils although such a review is important for a better understanding and prediction of the potential mobilization and toxicity. Therefore, this review summarizes the recent knowledge about REE contents and potential mobilization in different soil profiles in Germany. We found that the REE content tends to decrease in dependence on the parent material in the following order: Carbonatite > basalt > orthogneiss > clay slate > loess > sandstone > Pleistocene and Holocene sediments > organic material. Also, we used data of earlier studies, summarized and newly evaluated those data aiming to quantify the factors influencing the total REE content in German soil profiles. The contents of REEs in soil profiles of different parent material showed significant relations with content of clay, carbonate, organic matter, aluminium, iron, and manganese. Geochemical fractionation results suggest that the bioavailability of REEs is relatively low while the residual fraction is relatively high in German soils. In soils, where water fluctuations are important, the redox potential is a key factor controlling the mobilization of REEs also via related changes of pH.

摘要

稀土元素(REEs)在高科技产业、农业和医疗技术中的应用日益广泛,这导致它们被释放到土壤和水中,并转移到植物中,可能对人类健康和环境产生负面影响。可以通过REEs 的含量和地球化学行为以及土壤特性来评估它们在土壤中的毒性和潜在迁移性。然而,到目前为止,德国土壤中还没有对这些相互作用进行综述,尽管这种综述对于更好地理解和预测潜在的迁移性和毒性非常重要。因此,本综述总结了德国不同土壤剖面中 REE 含量和潜在迁移性的最新知识。我们发现,REE 含量随着母质的变化而逐渐减少,其顺序为:碳酸岩>玄武岩>正长岩>粘土片岩>黄土>砂岩>更新世和全新世沉积物>有机物质。此外,我们还利用了早期研究的数据,对这些数据进行了总结和重新评估,旨在量化影响德国土壤剖面中总 REE 含量的因素。不同母质土壤剖面中 REE 的含量与粘土、碳酸盐、有机质、铝、铁和锰的含量有显著关系。地球化学分馏结果表明,REE 在德国土壤中的生物可利用性相对较低,而残余态相对较高。在水波动较大的土壤中,氧化还原电位是控制 REE 迁移的关键因素,也通过相关的 pH 值变化来控制。

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